Forest Fuels and Fire Forest Fuels and Fire Behavior Behavior - - PowerPoint PPT Presentation
Forest Fuels and Fire Forest Fuels and Fire Behavior Behavior - - PowerPoint PPT Presentation
Forest Fuels and Fire Forest Fuels and Fire Behavior Behavior Rick Everett Rick Everett ESPM 134 ESPM 134 Spring 2008 Spring 2008 Where were going: Where were going: Fuels: What they are Fuels: What they are Fuel
Where we’re going: Where we’re going:
- Fuels: What they are
Fuels: What they are
- Fuel Classes
Fuel Classes
- Fuels & Fire Hazards
Fuels & Fire Hazards
- Fire Behavior
Fire Behavior
Fuels, Topography, Weather
Fuels, Topography, Weather
Flame & Flame front Characteristics
Flame & Flame front Characteristics
Spread Characteristics
Spread Characteristics
Fire Behavior Measurements
Fire Behavior Measurements
Fuels Classification Fuels Classification
Natural fuels
Natural fuels
From natural forest growth and death.
From natural forest growth and death.
Includes all leaf and branch materials
Includes all leaf and branch materials
Includes all duff, and litter
Includes all duff, and litter
Activity fuels
Activity fuels
Human
Human-
- caused
caused
Logging
Logging
Thinning
Thinning
Herbicide Use
Herbicide Use
Recreation
Recreation
Dead, downed & remnant
Dead, downed & remnant
All dead & down materials on the forest floor
All dead & down materials on the forest floor
Can be activity or natural
Can be activity or natural
Either sound or rotten
Either sound or rotten
Timelag Theory Timelag Theory
- Timelag Principle: wetting and drying of fuels
Timelag Principle: wetting and drying of fuels
Timelag: the amount of time required for a fuel to
Timelag: the amount of time required for a fuel to reach approximately 63% of the difference between reach approximately 63% of the difference between initial moisture content and equilibrium moisture initial moisture content and equilibrium moisture q content content
The 63% is a step function solution: 1
The 63% is a step function solution: 1-
- 1/e = 0.63, where
1/e = 0.63, where ‘e’ is the base of the natural log. ‘e’ is the base of the natural log.
Timelag Classification Timelag Classification
- The amount of fuel exposed to the atmosphere
The amount of fuel exposed to the atmosphere is related to fuel size is related to fuel size
Small diameter fuels have a large surface to area ratio
Small diameter fuels have a large surface to area ratio
Change rapidly with changes in temperature and humidity
Change rapidly with changes in temperature and humidity
Change rapidly with changes in temperature and humidity
Change rapidly with changes in temperature and humidity
Big diameter fuels have a small surface to volume
Big diameter fuels have a small surface to volume ratio ratio
Change slowly with changes in temperature and humidity
Change slowly with changes in temperature and humidity
- Timelag increases with increasing Fuel diameter
Timelag increases with increasing Fuel diameter
Fuel Classes Fuel Classes
- Classified by how quickly they can respond to changes in atmospheric
Classified by how quickly they can respond to changes in atmospheric conditions conditions
1-
- hour timelag fuels: 0.0 to 0.25”
hour timelag fuels: 0.0 to 0.25”
10
10-
- hour timelag fuels: 0.25 to 1.0”
hour timelag fuels: 0.25 to 1.0”
100
100-
- hour timelag fuels: 1.0 to 3.0”
hour timelag fuels: 1.0 to 3.0”
1000
1000-
- hour timelag fuels: 3.0 to 8.0”
hour timelag fuels: 3.0 to 8.0”
- Sampled using a line intercept transects (the “Brown Transect”
Sampled using a line intercept transects (the “Brown Transect”
- Sampled using a line intercept transects (the Brown Transect
Sampled using a line intercept transects (the Brown Transect
# of fuels intersecting 30m line can be converted to tons/unit area
# of fuels intersecting 30m line can be converted to tons/unit area
- Usually thought of as a “% fuel moisture”:
Usually thought of as a “% fuel moisture”:
If a 1 hour fuel stick is carrying only 10% of what is its tested maxima for
If a 1 hour fuel stick is carrying only 10% of what is its tested maxima for moisture, then the % fuel moisture is 10% moisture, then the % fuel moisture is 10%
- Easy to test, 0
Easy to test, 0-
- 100% scale
100% scale
- Live: 0
Live: 0 – – 200%; 200%;
Critical levels < 100 %
Critical levels < 100 % -
- half of the normal relative moisture
half of the normal relative moisture
Fuels: RAWS Data availability
- real time
- set for models
Fuels and Fire Hazards Fuels and Fire Hazards
Wildland Fuels are divided into 4 classes:
Wildland Fuels are divided into 4 classes:
Ground
Ground
Duff
Duff – – moist upper A horizon, decomposing litter moist upper A horizon, decomposing litter
Not a big player in fire behavior
Not a big player in fire behavior
Surface
Surface
All dead downed woody stuff, litter, grasses, herbs, shrubs
All dead downed woody stuff, litter, grasses, herbs, shrubs
dd dd
Ladder
Ladder
Fuels that provide vertical continuity from Surface to Crown
Fuels that provide vertical continuity from Surface to Crown
Crown
Crown
Overstory biomass
Overstory biomass Reductions of these fuels limit fire intensities
Reductions of these fuels limit fire intensities
Fuel treatments!
Fuel treatments!
Surface
Surface – – Ladder Ladder -
- Crown
Crown
Fire Behavior Fire Behavior
- 3 Interacting classes of influencing variables:
3 Interacting classes of influencing variables:
Fuels
Fuels
Topography
Topography
We ther
We ther
Weather
Weather
Fuels Fuels
- Already got it…
Already got it…
Topography Topography
Slope
Slope
Fires on slopes can
Fires on slopes can
Increase flame length,
Increase flame length,
Preheat upslope fuels
Preheat upslope fuels
These can increase intensity and rate
These can increase intensity and rate-
- of
- f-spread
spread y p p Terrain
Terrain
Topography can influence:
Topography can influence:
Slope (!)
Slope (!)
Diurnal air movement
Diurnal air movement
Aspect: fuels temperatures
Aspect: fuels temperatures
Physiography:
Physiography:
Chimneys, saddles, box canyons
Chimneys, saddles, box canyons
Chimney, slopes: NOT a good place to continue standing
Weather Weather
Temperature
Temperature
Relative Humidity
Relative Humidity
Precipitation
Precipitation
Atmospheric stability
Atmospheric stability
Vertical stability (inversions), advection
Vertical stability (inversions), advection
Winds & Windspeed
Winds & Windspeed
Winds & Windspeed
Winds & Windspeed
General
General – – broad scale pressure gradients broad scale pressure gradients
Foehn Winds: Santa Anas, Diablos
Foehn Winds: Santa Anas, Diablos
Local
Local
Sea breezes, land breezes, slope winds
Sea breezes, land breezes, slope winds
Fire Whorls
Fire Whorls
Critical: weather can change rapidly, changing fire behavior
Critical: weather can change rapidly, changing fire behavior rapidly rapidly
Weather Weather
Whorls: 10 to 1000’s m2, increase intensity eight-fold
Weather Weather
- Thunderstorms
Thunderstorms
Violent
Violent up/downdrafts up/downdrafts
Lightning
Lightning S i i d S i i d
Sometimes associated
Sometimes associated with cold fronts with cold fronts
Downdrafts often lead
Downdrafts often lead to violent, lateral front to violent, lateral front winds winds
Fire Movement Fire Movement
- 4 Processes: Convection, Conduction, Radiation,
4 Processes: Convection, Conduction, Radiation, Mass Transfer Mass Transfer
Convection:
Convection:
Conduction is the transfer of thermal energy (Q) from a
Conduction is the transfer of thermal energy (Q) from a
Conduction is the transfer of thermal energy (Q) from a
Conduction is the transfer of thermal energy (Q) from a region of higher temperature (A) to a region of lower region of higher temperature (A) to a region of lower temperature via direct molecular communication between temperature via direct molecular communication between mediums in direct physical contact without a flow of the mediums in direct physical contact without a flow of the material medium material medium
Convection Convection
- a mechanism of heat transfer occurring because
a mechanism of heat transfer occurring because
- f bulk motion (observable movement) of fluids
- f bulk motion (observable movement) of fluids
Air is a fluid…
Air is a fluid…
Radiation Radiation
Thermal radiation
Thermal radiation is electromagnetic is electromagnetic radiation emitted radiation emitted from the surface from the surface
- f an object
- f an object
which is due to which is due to the object's the object's temperature. temperature.
Infrared radiation
Infrared radiation
Colorado DNR
Mass Transfer Mass Transfer
- Phrase commonly used for physical processes
Phrase commonly used for physical processes that involve molecular and convective transport that involve molecular and convective transport
- f atoms and molecules within physical systems:
- f atoms and molecules within physical systems:
Moving stuff (usually gaseous) by convection
Moving stuff (usually gaseous) by convection
Moving stuff (usually gaseous) by convection
Moving stuff (usually gaseous) by convection
Molecules
Molecules
Sparks (glowing embers)
Sparks (glowing embers)
Flame Characteristics Flame Characteristics
Flame Height
Flame Height
Vertical distance flame extends
Vertical distance flame extends beyond fuels bed beyond fuels bed
Tough to measure…flames pretty
Tough to measure…flames pretty ephemeral ephemeral Flame Length
Flame Length
Distance from base of flame zone
Distance from base of flame zone to tip of continuous flames to tip of continuous flames to tip of continuous flames to tip of continuous flames
Used for intensity
Used for intensity
Highly variable: fluctuates due to
Highly variable: fluctuates due to wind, fire behavior, fuels wind, fire behavior, fuels
Flame Angle
Flame Angle
θ : angle between ground and
: angle between ground and average flame average flame
Influenced by winds, convection
Influenced by winds, convection
Flame Characteristics Flame Characteristics
Fire Spread Fire Spread
- Spread from a point ignition
Spread from a point ignition
Roughly elliptical shape
Roughly elliptical shape
Aligns central axis with
Aligns central axis with
Prevailing wind
Prevailing wind
Prevailing wind
Prevailing wind
Slope
Slope
Both
Both
Fire Spread Fire Spread
- Three main parts, used in perimeter and
Three main parts, used in perimeter and behavior descriptions: behavior descriptions:
Head (heading)
Head (heading)
Flames blown towards unburned fuels
Flames blown towards unburned fuels
Flames blown towards unburned fuels
Flames blown towards unburned fuels
Flank (flanking)
Flank (flanking)
Alternatively backing and heading
Alternatively backing and heading
Back (backing)
Back (backing)
Moves into the wind, or against a slope
Moves into the wind, or against a slope
Wildfire Spread Wildfire Spread
Wave (like waves in a pond)
Wave (like waves in a pond)
Low to Moderate Intensities
Low to Moderate Intensities
Spotting
Spotting
High intensity
High intensity
Easily places fire 1.5 miles away
Easily places fire 1.5 miles away
Fire Behavior Measurements Fire Behavior Measurements
Two Equations can be employed:
Two Equations can be employed:
Fireline intensity (I):
Fireline intensity (I):
I = 259L
I = 259L217
217 I is given in kW/m and
I is given in kW/m and
L is flame length in meters (m)
L is flame length in meters (m)
I L = 259
217 .
L is flame length in meters (m).
L is flame length in meters (m).
I = h
I = hωr
I is still kW/m
I is still kW/m
ω is fuel loading in kg/m
is fuel loading in kg/m2
r is the rate of spread in m/sec
r is the rate of spread in m/sec
This equation tends to overestimate; need to know difference between
This equation tends to overestimate; need to know difference between flaming combustion and smoldering combustion flaming combustion and smoldering combustion
Old standard (still used in structural stuff): BTU/foot/sec
Old standard (still used in structural stuff): BTU/foot/sec